Retrieval of UVB aerosol extinction profiles from the ground-based Langley Mobile Ozone Lidar (LMOL) system
-
Published:2022-04-22
Issue:8
Volume:15
Page:2465-2478
-
ISSN:1867-8548
-
Container-title:Atmospheric Measurement Techniques
-
language:en
-
Short-container-title:Atmos. Meas. Tech.
Author:
Lei Liqiao, Berkoff Timothy A., Gronoff GuillaumeORCID, Su Jia, Nehrir Amin R., Wu YonghuaORCID, Moshary Fred, Kuang ShiORCID
Abstract
Abstract. Aerosols emitted from wildfires are becoming one of the
main sources of poor air quality on the US mainland. Their extinction in UVB
(the wavelength range from 280 to 315 nm) is difficult to retrieve using simple
lidar techniques because of the impact of ozone (O3) absorption and the lack of
information about the lidar ratios at those wavelengths. Improving the
characterization of lidar ratios at the abovementioned wavelengths will enable aerosol monitoring with
different instruments and will also permit the correction of the aerosol impact on
O3 lidar data. The 2018 Long Island Sound Tropospheric Ozone Study
(LISTOS) campaign in the New York City region utilized a comprehensive set of
instruments that enabled the characterization of the lidar ratio for UVB aerosol
retrieval. The NASA Langley High Altitude Lidar Observatory (HALO) produced
the 532 nm aerosol extinction product along with the lidar ratio for this
wavelength using a high-spectral-resolution technique. The Langley Mobile
Ozone Lidar (LMOL) is able to compute the extinction provided that it has the
lidar ratio at 292 nm. The lidar ratio at 292 nm and the Ångström
exponent (AE) between 292 and 532 nm for the aerosols were retrieved by
comparing the two observations using an optimization technique. We evaluate
the aerosol extinction error due to the selection of these parameters,
usually done empirically for 292 nm lasers. This is the first known 292 nm
aerosol product intercomparison between HALO and Tropospheric Ozone Lidar
Network (TOLNet) O3 lidar. It also provides the characterization of the
UVB optical properties of aerosols in the lower troposphere affected by
transported wildfire emissions.
Funder
New York State Energy Research and Development Authority NOAA Center for Earth System Sciences and Remote Sensing Technologies
Publisher
Copernicus GmbH
Subject
Atmospheric Science
Reference65 articles.
1. Aggarwal, M., Whiteway, J., Seabrook, J., Gray, L., Strawbridge, K., Liu, P., O'Brien, J., Li, S.-M., and McLaren, R.: Airborne lidar measurements of aerosol and ozone above the Canadian oil sands region, Atmos. Meas. Tech., 11, 3829–3849, https://doi.org/10.5194/amt-11-3829-2018, 2018. 2. Andreae, M. O. and Merlet, P.: Emission of trace gases and aerosols from
biomass burning, Global Biogeochem. Cy., 15,
955–966, https://doi.org/10.1029/2000GB001382, 2001. 3. Bais, A. F., Zerefos, C. S., Meleti, C., Ziomas, I. C., and Tourpali, K.:
Spectral measurements of solar UVB radiation and its relations to total
ozone, SO2, and clouds, J. Geophys. Res.-Atmos., 98,
5199–5204, https://doi.org/10.1029/92jd02904, 1993. 4. Berkoff, T., Gronoff, G., Sullivan, J., Nino, L., Carrion, W., Twigg, L., Sparrow, J., Knepp, T., Tully, D., Chaffe, M., Babich, P., Valin, L., and Szykman, J.: Ozone Lidar Observations During the Long Island Sound Tropospheric Ozone Study, LISTOS Meeting, Albany, New York, 11 April 2019, https://www.nescaum.org/documents/listos/presentations-from-listos-meeting-albany-ny/berkoff.pdf (last access: 20 April 2022), 2019. 5. Brooks, I. M.: Finding Boundary Layer Top: Application of a Wavelet
Covariance Transform to Lidar Backscatter Profiles, J. Atmos. Ocean. Tech.,
20, 1092–1105, https://doi.org/10.1175/1520-0426(2003)020<1092:FBLTAO>2.0.CO;2, 2003.
Cited by
2 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|